Heat flow and quantity of methane deduced from a gas hydrate field in the vicinity of the Dnieper Canyon, northwestern Black Sea

Heat flow and quantity of methane deduced from a gas hydrate field in the vicinity of the Dnieper Canyon, northwestern Black Sea

Seismic reflection data document for the first time the existence of a BSR in a limited area west of the Dnieper Canyon in the northwestern Black Sea. Seismic wide-angle data suggest that gas hydrates occupy in average 15+/-2% of the pore space in a zone of 100 m in thickness. A conservative quantif...

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Veröffentlicht in:Geo-marine letters 2004-07, Vol.24 (3), p.182-193
Hauptverfasser: L dmann, Thomas, Wong, HowKin, Konerding, Philipp, Zillmer, Matthias, Petersen, J rg, Fl h, Ernst
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Sprache:eng
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Canyons
Gas hydrates
Heat flow
Hydrates
Marine
Methane
Seismology
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creator L dmann, Thomas
Wong, HowKin
Konerding, Philipp
Zillmer, Matthias
Petersen, J rg
Fl h, Ernst
description Seismic reflection data document for the first time the existence of a BSR in a limited area west of the Dnieper Canyon in the northwestern Black Sea. Seismic wide-angle data suggest that gas hydrates occupy in average 15+/-2% of the pore space in a zone of 100 m in thickness. A conservative quantification of the amount of methane associated with this gas hydrate occurrence is about 12+/-3times10
doi_str_mv 10.1007/s00367-004-0169-y
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source Springer Nature - Complete Springer Journals
subjects Canyons
Gas hydrates
Heat flow
Hydrates
Marine
Methane
Seismology
title Heat flow and quantity of methane deduced from a gas hydrate field in the vicinity of the Dnieper Canyon, northwestern Black Sea
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